| 安家营子金矿田矿床及同源岩体同位素地球化学 |
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| 引用本文： | 谢锡才,王义文,董万成,吕晓东,刘晓利.安家营子金矿田矿床及同源岩体同位素地球化学[J].地质与资源,1997,6(3):171-182. |
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| 作者姓名： | 谢锡才 王义文 董万成 吕晓东 刘晓利 |
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| 作者单位： | 1. 东北大学黄金学院地质系;2. 中国有色金属工业总公司吉林矿产地质研究所;3. 赤峰市喀喇沁旗金蟾山金矿 |
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| 摘 要： | S、Pb、C、O和H同位素研究表明,安家营子矿田金矿成矿物质主要来自深部岩浆源,成矿流体为再平衡岩浆水.与金矿有关的安家营子二长花岗岩体为下地壳重熔成因,属金铜系列花岗岩类.金矿成矿年龄为120~130Ma.
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| 关 键 词： | 稳定同位素 成矿物质来源 金铜系列花岗岩 成矿年龄 |
| 收稿时间： | 1997-05-16 |
THE ISOTOPIC GEOCHEMISTRY OF ORE DEPOSITS AND COGNATE ROCKS IN ANJIAYINGZI GOLD FIELD |
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| Xie Xicai,Wang Yiwen,Dong Wancheng,Lǜ Xiaodong,Liu Xiaoli.THE ISOTOPIC GEOCHEMISTRY OF ORE DEPOSITS AND COGNATE ROCKS IN ANJIAYINGZI GOLD FIELD[J].Geology and Resources,1997,6(3):171-182. |
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| Authors: | Xie Xicai Wang Yiwen Dong Wancheng Lǜ Xiaodong Liu Xiaoli |
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| Institution: | 1. Institute of Gold Technology, Northeast University, Shenyang;2. Jilin Research Institute of Mineral Resources and Geology, CNNC;3. Jinchanshan Gold Mine of Kalaqin County, Chifeng City |
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| Abstract: | Study on the S,Pb,C,O,H and Sr isotopes shows that:(1)the ore forming substances of Anjiayingzi gold field were mianly derived from deep magmatic source;(2)the ore forming fluid was re equilibrated magmatic water;and(3)Anjiayingzi adamellite mass related to gold deposits was derived from remelting lower crust rocks,it should belong to Au Cu series granitoidThe minerogenetic ages of gold deposits are 120～130Ma |
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| Keywords: | stable isotope ore forming substance Au Cu series granitoid minerogenetic ages |
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